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A systematic low-temperature neutron diffraction study of the RBa<sub>2</sub>Cu<sub>3</sub>O<sub>x</sub>(R=yttrium and rare earths; x=6 and 7) compounds

111

Citations

11

References

1994

Year

Abstract

The crystal structures of RBa<sub>2</sub>Cu<sub>3</sub>O<sub>x</sub> (R=Y and rare earths; x=6 and 7) ceramic materials were investigated at 10 K by neutron diffraction and consistently analysed concerning systematic trends. Other than for non-superconducting PrBa<sub>2</sub>Cu<sub>3</sub>O<sub>7</sub> the lattice parameters and most interionic distances exhibit the well known lanthanide contraction behaviour, i.e., a linear relationship with the ionic radii of trivalent rare-earth ions. The only exceptions are associated with the apex oxygen O(1) ions: the chain copper Cu(1)-O(1) distances are constant within error limits, and the plane copper Cu(2)-O(1) distances are increasing across the rare-earth series. The much stronger increase of the distance Cu(2)-O(1) in the RBa<sub>2</sub>Cu<sub>3</sub>O<sub>6</sub> series compared to the RBa <sub>2</sub>Cu<sub>3</sub>O<sub>7</sub> series can be explained by the increase of T<sub>c</sub> from 90 K for YbBa<sub>2</sub>Cu<sub>3</sub>O<sub>7</sub> to 96 K for NbBa<sub>2</sub>Cu<sub>3</sub>O<sub>7</sub>. The smaller distance Cu(1)-O(1) for the RBa<sub>2</sub>Cu<sub>3</sub>O<sub>6</sub> series compared to the RBa<sub>2</sub>Cu<sub>3</sub>O<sub>7</sub> series may be related to the suggested double-well potential of the apical oxygen ion. For some interionic distances of PrBa<sub>2</sub>Cu<sub>3</sub>O<sub>7</sub> approximately parallel to the h direction (i.e., the chain direction) we determine by extrapolation a valence of +3.4 for the Pr ions. This indicates for PrBa<sub>2</sub>Cu <sub>3</sub>O<sub>7</sub> a highly anisotropic 4f-CuO<sub>2</sub> valence band hybridization. An important structural property with respect to the superconductivity is the puckering of the CuO<sub>2</sub> planes: the superconductivity is lost when the puckering angle exceeds a critical value of about 167.3°.

References

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